The active structure of the eastern flank of the Central Range in Taiwan
博士 === 國立中央大學 === 地球科學學系 === 107 === Taiwan Island is an active orogenic belt, as a result of the Philippine Sea plate colliding with the Eurasian plate with a speed of around 8.2 cm/yr. The rapidly convergent rate results in significant crustal deformation and ongoing mountain building process. Bot...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Others |
| Language: | zh-TW |
| Published: |
2019
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| Online Access: | http://ndltd.ncl.edu.tw/handle/545fwm |